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在压力下通过醋酸钾插层对高岭石羟基表面进行改性

Modification of the Kaolinite Hydroxyl Surfaces through Intercalation with Potassium Acetate under Pressure.

作者信息

Frost RL, Kristof J, Paroz GN, Kloprogge JT

机构信息

Centre for Instrumental and Developmental Chemistry, Queensland University of Technology, 2 George Street, Brisbane, Queensland, 4001, Australia

出版信息

J Colloid Interface Sci. 1998 Dec 15;208(2):478-486. doi: 10.1006/jcis.1998.5855.

Abstract

Kaolinite hydroxyl surfaces have been modified upon intercalation with potassium acetate under a range of conditions. Modification is observed by changes in the hydroxyl stretching region using Raman and infrared spectroscopy. Upon the intercalation of low defect kaolinite with potassium acetate under a pressure of 20 bars and 220 degreesC, the Raman spectra showed additional bands at 3590, 3603, and 3609 cm-1. The DRIFT spectra of this intercalate showed new bands at 3595 and 3605 cm-1. These bands are attributed to the inner surface hydroxyls hydrogen bonded to the acetate anion. Intercalation under 20 bars pressure at 220 degreesC caused the differentiation of the inner surface hydroxyl groups, resulting in these additional bands. By using milder conditions of 2 bars and at 120 degreesC, additional Raman bands were found at 3592, 3600, and 3606 cm-1. If the kaolinite was intercalated at 1 bar and 100 degreesC, a new broad Raman band was found at 3605 cm-1. It is proposed that the effect of intercalation of the low defect kaolinite under pressure caused the kaolinite to become disordered and this disordering was dependent upon the temperature of intercalation. Copyright 1998 Academic Press.

摘要

在一系列条件下,高岭石的羟基表面在与醋酸钾插层时会发生改性。通过拉曼光谱和红外光谱在羟基伸缩区域的变化来观察改性情况。在20巴压力和220℃下,将低缺陷高岭石与醋酸钾插层时,拉曼光谱在3590、3603和3609 cm-1处出现了额外的谱带。该插层物的漫反射红外傅里叶变换光谱(DRIFT)在3595和3605 cm-1处出现了新的谱带。这些谱带归因于与醋酸根阴离子形成氢键的内表面羟基。在220℃、20巴压力下进行插层导致内表面羟基基团发生分化,从而产生了这些额外的谱带。在2巴和120℃的温和条件下,在3592、3600和3606 cm-1处发现了额外的拉曼谱带。如果高岭石在1巴和100℃下插层,则在3605 cm-1处发现一个新的宽拉曼谱带。有人提出,在压力下低缺陷高岭石插层的影响导致高岭石变得无序,且这种无序取决于插层温度。版权所有1998年学术出版社。

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